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Climate change, typhoons, and floods on the Ara River, central Japan.

机译:日本中部荒河上的气候变化,台风和洪水。

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摘要

Portions of the flood history of the Ara River in central Japan are documented using data from the 20th century, the historical past, and the geological past (the Holocene). In the 20 th century, annual maximum floods were found to have been larger from 1910–1950 and 1982–1998, and smaller from 1952–1981 (no data for 1951). The dates of shifts in flood magnitudes are close to those found for shifts in flood magnitudes in the Upper Mississippi Valley of the U.S., and for major shifts in the dominance of differing phases of the PDO (Pacific Decadal Oscillation) and the ENSO. During the Little Ice Age, historical documentary records indicate that floods were frequent but showed decadal-scale variations with higher (lower) frequencies during cooler (warmer) periods and during periods dominated by El Niño (La Niña) phases of the ENSO and positive (negative) phases of the PDO. For the Holocene, reconstruction of a part of the flood record based on the analysis of terrace and floodplain gravels indicates that floods were generally larger during the early to mid-Holocene but variable during the mid- to late Holocene with generally larger (smaller) floods during colder (warmer) periods. Flood magnitudes also showed a weak relationship with El Niño activity after the mid-Holocene. The Ara River Holocene flood record showed similarities in the timing of periods of larger (smaller) floods with significant periods of fluvial activity in Japan, Europe, and the U.S. As typhoons are the main cause of large floods in the 20th century and the historical past, trends in the magnitudes and frequencies of floods on the Ara River at various time scales are linked to similar-scale trends in the behavior of typhoons in the Northwestern Pacific Ocean. This typhoon and flood behavior can be related to climate change through shifts in the persistence of atmospheric circulation patterns and phenomena such as the ENSO and PDO. It is therefore suggested that shifts in the global climate at various time-scales throughout the Holocene have been the main driving force for changes in the behavior of typhoons and, consequently, in the Ara River flood regime.
机译:日本中部地区的阿拉河洪水历史的某些部分使用20世纪以来的数据,历史历史和地质历史(全新世)进行了记录。在20世纪,发现年度最大洪水在1910年至1950年和1982年至1998年之间较大,而在1952年至1981年之间较小(1951年没有数据)。洪水幅度的变化日期与美国密西西比河上游流域的洪水幅度变化以及PDO(太平洋年代际涛动)和ENSO不同阶段的主导地位发生重大变化的日期相近。在小冰河时期,历史文献记录表明,洪水频发,但在较冷的(较暖)时期以及ENSO的厄尔尼诺(拉尼娜)阶段和正(否)阶段。对于全新世,根据阶地和洪泛区砾石的分析重建一部分洪灾记录表明,在全新世早期至中期,洪灾通常较大,而在全新世中期至晚期,洪灾变化较大,洪水一般较大(较小)在较冷的时期。全新世中期以后,洪水强度与厄尔尼诺现象之间的关系较弱。阿拉河全新世洪水记录显示,在日本,欧洲和美国,较大(较小)洪水和大量河流活动周期的时间点相似,因为台风是20世纪20年代大洪水的主要原因。上世纪和历史的过去,阿拉河在不同时间尺度上洪水的数量和频率趋势与西北太平洋台风行为的相似尺度趋势相关。这种台风和洪水行为可以通过改变大气环流模式和诸如ENSO和PDO之类的现象的持久性与气候变化有关。因此,有人提出,在全新世期间,全球气候在各个时间尺度上的变化已成为改变台风行为,进而改变阿拉河洪水制度的主要动力。

著录项

  • 作者

    Grossman, Michael Joel.;

  • 作者单位

    The University of Wisconsin - Madison.;

  • 授予单位 The University of Wisconsin - Madison.;
  • 学科 Physical Geography.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 285 p.
  • 总页数 285
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 自然地理学;
  • 关键词

  • 入库时间 2022-08-17 11:44:44

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